本文描述了一种以MODIS图像反演陆地大气气溶胶光学厚度的算法,它是基于6S大气辐射传输模型计算的查找表(LUT),并利用地面的暗目标自动反演陆地大气气溶胶光学厚度的方法.利用该算法给出了我国江西省中部地区的2001年10月19日550 nm波长的平均大气气溶胶光学厚度(0.19),这与从国家气象档案馆获得的该地区的气象能见度计算结果有较好的一致性.
参考文献
[1] | 毛节泰,李成才等.MODIS卫星遥感北京地区气溶胶光学厚度及与地面光度计遥感的对比[J].应用气象学报,2002,13(U01):127-135 |
[2] | Vermote E F, Tanre D, Deuze J L, et al. Second simulation of the satellite signal in the solar spectrum, 6S: an overview [J]. IEEE Trans. Geosci. Remote Sens., 1997, 35:675-686 |
[3] | Fraser R S, Kanfman Y J. The relative importance of scattering and absorption in remote sensing [J]. IEEE Trans. Geosci. Remote Sens., 1985, 23:625-633 |
[4] | Lee T Y, Kaufman Y J. The effect of surface non-Lambertianity on remotesensing of ground reflectance and vegetation index [J]. IEEE J. Geos. Rem. Sens., 1986(a), GE-24:699-708 |
[5] | Barnes W L, Pagano T S, Salomonson V V. Prelaunch characteristics of the moderate resolution imaging spectroradiometer (MODIS) on EOS-AM1 [J]. IEEE Trans. Geosci Remote Sensing, 1998, 36(4): |
[6] | Kaufman YJ, Wald A, Remer L A, et al. Remote sensing of aerosol over the continents with the aid of a 2.2 mm channel [J]. IEEE Trans. Geosci. Remote Sensing., 1997, 35:1286-1298 |
[7] | Kanfman Y J, et al. Algorithm for antomatic atmospheric corrections to visible and near-IR satellite imagery [J].Int. J. Rem. Sens., 1988, 9:1357-1381 |
[8] | Zagolski F, Gastellu-Etchegorry J P. Atmospheric corrections of AVIRIS images with a procedure based on the inversion of the 5S model [J]. Int. J. Rem. Sens., 1995, 16:3115-3146 |
[9] | 国家地质总局航空物探大队遥感室.<地球资源卫星象片图集>[M].北京:地质出版社 |
[10] | Ouaidrari O, Vermote E F. Operational atmospheric correction of landsat TM data [J]. Remote Sens. Environ,1999, 70:4-15 |
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